Abstract:
In some serious environmental constraints, soil salinity is a worldwide major issue for
crop production and soil declination. Salinity in Pakistan has covered 6.68 million
hectares area of cultivated land and further out of 6.68 million hectares 56% area is
covered by saline sodic. The soil salinity causes hindrance in the availability of very
essential macronutrients like phosphorus. The relation between phosphorus uptake and
soil salinity is a complex phenomenon. With the aim to calculate phosphorus (P) fractions
and to maximize P bioavailability in wheat crop, a series of pot and field experiments
were conducted in normal and salt affected soils.
In 1st incubation study rate of P was selected on the basis of plant available P at different
time intervals from three different rates (200, 400 and 600 mg kg-1 of soil) of P fertilizer.
Results revealed that among different fractions of P (bound and bioavailable), maximum
Olsen-P was found 12.18 mg kg-1 in PROKA soil (saline sodic), 9.225 mg kg-1 in PARS
soil (saline) and 9.125 mg kg-1 in UAF soil (normal), when P was applied at 400 mg kg-1
of soil. Selected rate of P fertilizer (400 mg kg-1) was used in 2nd incubation study with
different organic amendments [farmyard manure (FYM), poultry manure (PM), crop
residue (CR)] and sewage sludge (SS) for the determination of P fractions at different
time intervals. Plant available Olsen-P fraction significantly increased after 90 days of
incubation in all soils (normal, saline sodic, saline) with amendments FYM and PM but
not as much with amendments CR and SS at P application level 400 mg kg-1 of soil.
Overall, Olsen-P was increased maximum with PM (23.2, 21.7 and 19.4 mg kg-1) and
FYM (20.6, 17.6 and 20.6 mg kg-1) as compare with SS (14.3, 15.5 and 15.7 mg kg-1) and
CR (12.9, 14.4 and 14.0 mg kg-1) in normal, saline sodic and saline soils, respectively. To
evaluate the effect of P rate (400 mg kg-1) selected from 1st study and organic
amendments (FYM and PM) selected from 2nd study, A subsequent pot experiment was
conducted in normal (UAF) and salt-affected (PROKA and PARS) soils. Results showed
a significant effect on wheat growth, yield, physiological, chemical and biochemical
parameters by combined application of P + PM in all soils. On the basis of these
parameters, P + PM remained as best in normal and salt-affected soils with order of
normal>saline>saline sodic.
In pot experiment, maximum level of grain yield (24%), photosynthesis (37%), protein
(20%), fat (40%), starch (41%) and maximum reduction in polyphenol (47%) were
observed by combined application of P + PM, over control. Highest level of P in root
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(53%), shoot (57%) and grain (121%) was found in wheat plant grown in normal soil
while maximum level of Olsen-P (99%) was observed in saline sodic soil by P+PM
treatment, over control. In field experiment, results showed that growth parameters such
as plant height, root dry weight and 1000 grain weight were increased maximum with PM
+ P treatment in all soils. Photosynthetic parameters also affected significantly in all three
types of soils by combined application of PM + P. Significant effect of combined
application of P fertilizer and PM was recorded in case of P concentration in wheat root,
shoot and grain in all soils. Biochemical parameters such as protein, fat, fiber, ash, starch
and polyphenols were also affected significantly with treatment PM + P. Overall these
experimental results showed that P fertilizer applied with PM, not only improved wheat
growth, yield and physiology but also improved grain nutritional value and P uptake in
both type of soils (normal and salt-affected). Reduction in adverse effect of soil salinity
was also observed by integration of chemical fertilizers and organic amendments.